{"id":1286,"date":"2025-07-10T09:09:23","date_gmt":"2025-07-10T09:09:23","guid":{"rendered":"https:\/\/icewalk.it\/rundhoecker\/"},"modified":"2026-01-28T13:17:40","modified_gmt":"2026-01-28T13:17:40","slug":"rundhoecker","status":"publish","type":"page","link":"https:\/\/icewalk.it\/de\/rundhoecker\/","title":{"rendered":"Rundh\u00f6cker"},"content":{"rendered":"

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Rundh\u00f6cker<\/h1>\n

 <\/p>\n

Die Handschrift der Gletscher <\/span><\/h3>\n

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Rundh\u00f6cker sind glattgeschliffene, l\u00e4ngliche Felsr\u00fccken, die w\u00e4hrend der Eiszeiten durch die Gletscher geformt wurden. Ihre asymmetrische Gestalt zeigt die Wirkung zweier Prozesse: Auf der dem Gletscher zugewandten Seite dominierte die Abrasion<\/b> \u2013 das Eis und die eingeschlossenen Gesteinstr\u00fcmmer polierten den Fels zu glatten Oberfl\u00e4chen mit sichtbaren Gletscherschrammen. Auf der Talseite dagegen f\u00fchrte der Prozess des Plucking<\/b> zum Herausbrechen von Gesteinsst\u00fccken: Wasser drang in Spalten ein, gefror, dehnte sich aus und sprengte die Felsen.<\/span><\/p>\n

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H\u00e4ufig wachsen auf diesen Felsen die auff\u00e4lligen Landkartenflechten<\/b> (Rhizocarpon geographicum)<\/i>. Ihr gr\u00fcnlich-gelber Thallus mit dunklen Flecken erinnert an eine Landkarte. Da sie extrem langsam wachsen \u2013 nur wenige Zehntel Millimeter pro Jahr \u2013 gelten sie als n\u00fctzliche Indikatoren f\u00fcr das Alter exponierter Felsen, auch wenn sie keine exakten Datierungen erlauben.<\/span><\/p>\n

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Wissenswertes<\/span><\/h5>\n

<\/span><\/h3>\n

Der Begriff roche moutonn\u00e9e<\/i> wurde im 18. Jahrhundert vom Naturforscher Horace-B\u00e9n\u00e9dict<\/i> de Saussure gepr\u00e4gt. Die Bezeichnung erinnert an die welligen Per\u00fccken der franz\u00f6sischen Aristokratie, die mit Schafsfett (mouton) in Form gehalten wurden.<\/span><\/h3>\n

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Tappeinerweg, Meran.<\/span><\/p>\n

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Rundh\u00f6cker, Gletscherschrammen und gro\u00dfe Findlinge<\/b> sind bleibende Spuren der Gletscher. Sie finden sich auch weitab heutiger Gletscherregionen, etwa die Schrammen an der Tappeinerpromenade in Meran oder der ber\u00fchmte \u201eAlter Schwede\u201c im Hamburger Hafen, der vom skandinavischen Inlandeis dorthin transportiert wurde.<\/span><\/p>\n

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Findling: Hamburger Hafen, Deutschland.<\/span><\/p>\n

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Sandhamn, Schweden.<\/span><\/p>\n

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Yosemite-Nationalpark, USA.<\/span><\/p>\n

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